Popov (crater)

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Popov
Popov LROC.jpg
LRO image
Coordinates 17°12′N99°42′E / 17.2°N 99.7°E / 17.2; 99.7 Coordinates: 17°12′N99°42′E / 17.2°N 99.7°E / 17.2; 99.7
Diameter 71.4 km
Depth unknown
Colongitude 261° at sunrise
Eponym Aleksander S. Popov,
Cyril Popov [1]

Popov is a crater on the far side of the Moon, just beyond the eastern limb. It measures approximately 71.4 kilometers (44.4 miles) in diameter and is located along the very edge of the area of surface that is sometimes brought into view of the Earth during periods of favorable libration and illumination. However even at such times it is not prominent and can only be viewed edge-on. [2]

Impact crater Circular depression on a solid astronomical body formed by a hypervelocity impact of a smaller object

An impact crater is an approximately circular depression in the surface of a planet, moon, or other solid body in the Solar System or elsewhere, formed by the hypervelocity impact of a smaller body. In contrast to volcanic craters, which result from explosion or internal collapse, impact craters typically have raised rims and floors that are lower in elevation than the surrounding terrain. Impact craters range from small, simple, bowl-shaped depressions to large, complex, multi-ringed impact basins. Meteor Crater is a well-known example of a small impact crater on Earth.

Moon Earths natural satellite

Earth's Moon is an astronomical body that orbits the planet and acts as its only permanent natural satellite. It is the fifth-largest satellite in the Solar System, and the largest among planetary satellites relative to the size of the planet that it orbits. The Moon is, after Jupiter's satellite Io, the second-densest satellite in the Solar System among those whose densities are known.

Earth Third planet from the Sun in the Solar System

Earth is the third planet from the Sun and the only astronomical object known to harbor life. According to radiometric dating and other sources of evidence, Earth formed over 4.5 billion years ago. Earth's gravity interacts with other objects in space, especially the Sun and the Moon, Earth's only natural satellite. Earth orbits around the Sun in 365.26 days, a period known as an Earth year. During this time, Earth rotates about its axis about 366.26 times.

Contents

Description

This crater lies due south of Dziewulski, and the crater chain designated Catena Dziewulski passes just to the northeast of Popov's outer rim. Just to the southeast of Popov lies Möbius, and the two are joined together by a smaller crater that lies along the south-southeast rim of Popov. To the southwest lies the crater Ginzel and Mare Marginis.

Dziewulski (crater) lunar crater

Dziewulski is a lunar impact crater on the far side of the Moon. It lies between the craters Edison to the north and Popov to the south. The outer rim of this crater has been considerably worn by impacts, particularly along the southwest quadrant where the satellite crater Dziewulski Q overlies the rim and the interior floor. The northern rim is also heavily disrupted, and several small crater lie along the southeast rim. The interior floor and surrounding terrain has been resurfaced.

Möbius (crater) lunar crater

Möbius is a lunar impact crater that is located on the Moon's far side, beyond the eastern limb and northeast of the Mare Marginis. It lies less than one crater diameter to the northwest of the larger, 90-km-diameter Hertz, and just to the southeast of Popov. To the north of Mobius is the crater chain designated Catena Dziewulski, which takes its name from the crater Dziewulski to the north-northwest.

Ginzel (crater) lunar crater

Ginzel is a lunar impact crater that is located on the far side of the Moon, just beyond the eastern limb. It is named after the Austrian astronomer Friedrich Karl Ginzel. It lies at the eastern edge of the Mare Marginis, in a region of the surface that is sometimes brought into sight of the Earth due to libration. To the north-northeast of Ginzel is the crater Popov, and Dreyer lies due south.

Popov is a worn crater with a damaged outer rim that is little more than a circular, jumbled series of ridges in the surface. Several small craterlets lie along the rim and inner wall, particularly along the western side. The interior floor is otherwise relatively level and nearly without any features.

It is named after Russian physicist Alexander Stepanovich Popov, who is considered to be the inventor of radio in his homeland and eastern European countries. [3] [4]

Alexander Stepanovich Popov Russian physicist

Alexander Stepanovich Popov was a Russian physicist, who was one of the first persons to invent a radio receiving device.

Invention of radio aspect of history relating to the invention of radio

The invention of radio communication, although generally attributed to Guglielmo Marconi in the 1890s, spanned many decades, from theoretical underpinnings, through proof of the phenomenon's existence, development of technical means, to its final use in signalling.

Satellite craters

Oblique Apollo 14 image Popov crater AS14-71-9889.jpg
Oblique Apollo 14 image

By convention these features are identified on lunar maps by placing the letter on the side of the crater midpoint that is closest to Popov.

SatelliteLatitudeLongitudeDiameterRef
D17.8° N102.6° E17.48 km WGPSN
W19.1° N97.8° E26.3 km WGPSN

See also

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Challis (crater) lunar crater

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References

  1. Patrick Moore; Robin Rees. (2011). Patrick Moore's Data Book of Astronomy (2nd ed.). Cambridge University Press. p. 72. ISBN   9781139495226.
  2. "Popov (crater)" . Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program.
  3. Schmadel, Lutz D. (2007). "(3074) Popov". Dictionary of Minor Planet Names – (3074) Popov. Springer Berlin Heidelberg. p. 253. doi:10.1007/978-3-540-29925-7_3075. ISBN   978-3-540-00238-3.
  4. Smith-Rose, Reginald Leslie (2013). "Alexandr Popov". Encyclopædia Britannica Online. Encyclopædia Britannica, Inc. Retrieved 6 November 2013.
Ewen Whitaker British astronomer

Ewen Adair Whitaker was a British-born astronomer who specialized in lunar studies. During World War II he was engaged in quality control for the lead sheathing of hollow cables strung under the English Channel as part of the "Pipe Line Under The Ocean" Project (PLUTO) to supply gasoline to Allied military vehicles in France. After the war, he obtained a position at the Royal Greenwich Observatory working on the UV spectra of stars, but became interested in lunar studies. As a sideline, Whitaker drew and published the first accurate chart of the South Polar area of the Moon in 1954, and served as director of the Lunar Section of the British Astronomical Association.

NASA space-related agency of the United States government

The National Aeronautics and Space Administration is an independent agency of the United States Federal Government responsible for the civilian space program, as well as aeronautics and aerospace research.

United States Geological Survey Scientific agency of the United States government

The United States Geological Survey is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization has four major science disciplines, concerning biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility.